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Geology
Article: pp. 487–490 | Full Text | PDF (369K)
Direct dating of Archean microbial ichnofossils
1. Department of Earth Sciences, University of Western Ontario, London, Ontario N6A 5B7, Canada, 2. Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada, 3. Centre for Geobiology and Department of Earth Science, University of Bergen, Allegaten 41, 5007 Bergen, Norway, 4. Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada, 5. Scripps Institution of Oceanography, University of California, La Jolla, California 92093-0225, USA, 6. Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada, 7. Geological Survey of Western Australia, 100 Plain Street, East Perth, Western Australia 6004, Australia
Well-preserved Archean pillow lavas from the ca. 3.35 Ga Euro Basalt of the Pilbara Craton, Western Australia, contain micron-sized tubular structures mineralized by titanite (CaTiSiO4) with residual organic carbon preserved along their margins. Direct U-Pb dating of titanite in the tubular structures demonstrates an Archean age. These tubular microstructures are identical to microbial ichnofossils in modern basalts, ophiolites, and greenstone belts, and are interpreted as a biogenic signature in these ancient rocks. Microbial colonization of basaltic glass thus appears to have been part of a deep subsurface biosphere established early in Earth's history.
Keywords: early life, greenstone belt, Pilbara Craton, geochronology, ichnofossil, astrobiology
Received: 10 December 2006; Revised: 22 January 2007; Accepted: 24 January 2007
DOI: 10.1130/G23534A.1
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